Soil Data Explorer - BAXTER

Official Series Description

Lab Data Summary

Aggregate lab data for the BAXTER soil series. This aggregation is based on all pedons with a current taxon name of BAXTER, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to BAXTER were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
116A	59ID11	1959AR06311	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.8267,-91.7746
116A	59ID23	1959AR06323	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.8267,-91.7746
116A	60ID33	1960AR06333	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	35.8267,-91.7746
116A	63WS24	1963AR14324	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.1999813,-93.950141
116A	64BN02	1964AR00702	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.2875,-93.9489
116A	68BO04	1968AR00904	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.49389,-93.22722
116A	M9901725	1999MO017025	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.3628693,-89.9645844
122	WS8007	1980IN175007	Baxter	2	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.4216833,-86.1052389
122	WS8009	1980IN175009	Baxter	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	38.419925,-86.1129694
122	73KY-047-006	77KY047001	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	36.7425,-87.6407111
122	87KY-163-002	87KY-163-002	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	37.915062,-86.0641327
n/a	73KY-221-012	73KY-221-012	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	75KY-227-001	75KY-227-001	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	75KY-227-018	75KY-227-018	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a
n/a	83KY-099-001	83KY-099-001	Baxter	4	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BAXTER soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BAXTER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-06) and snapshot of SC database (updated 2023-10-02).

Select annual climate data summaries for the BAXTER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

Geomorphic description summaries for the BAXTER series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2023-10-04).

Competing Series

Soil series competing with BAXTER share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-06) and snapshot of the SC database (updated 2023-10-02).

Select annual climate data summaries for the BAXTER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

Geomorphic description summaries for the BAXTER series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records (updated 2023-10-04).

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BAXTER, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database (updated 2023-10-02).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. KY-2010-09-10-12 | Butler and Edmonson Counties -

   Relationship of soils to topography and underlying material in the Baxter-Pembroke-Fredonia association (Soil Survey of Butler and Edmonson Counties, Kentucky).

2. KY-2012-01-26-01 | Adair County - April 1964

   Diagram of the Westmoreland-Caneyville-Baxter association in Adair County (Soil Survey of Adair County, Kentucky; April 1964).

3. KY-2012-01-26-02 | Adair County - April 1964

   Diagram of the Baxter-Christian-Bewleyville association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

4. KY-2012-01-26-06 | Adair County - April 1964

   Geological cross section of Adair County showing the relationship of the soils to the underlying rocks (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

5. KY-2012-01-26-41 | Breckinridge and Meade Counties - 2001

   Typical relationship of soils to topography and the underlying material in the Crider-Fredonia general soil map unit (Soil Survey of Breckinridge and Meade Counties, Kentucky; 2001).

6. KY-2012-01-26-42 | Breckinridge and Meade Counties - 2001

   Typical relationship of soils to topography and the underlying material in the Baxter-Hammack-Crider general soil map unit (Soil Survey of Breckinridge and Meade Counties, Kentucky; 2001).

7. KY-2012-01-27-11 | Caldwell County - September 1966

   Typical pattern of soils and underlying materials in association 5 (Soil Survey of Caldwell County, Kentucky; September 1966).

8. KY-2012-01-27-12 | Caldwell County - September 1966

   Typical pattern of soils and underlying materials in association 6 (Soil Survey of Caldwell County, Kentucky; September 1966).

9. KY-2012-01-27-51 | Crittenden County - September 1988

   Relationship of soils to topography and underlying material in the Baxter-Hammack-Nicholson map unit (Soil Survey of Crittenden County, Kentucky; September 1988).

10. KY-2012-01-30-17 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Baxter-Crider general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

11. KY-2012-01-30-20 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Nolichucky-Canmer general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

12. KY-2012-02-01-04 | Livingston County - September 1993

    Relationship of soils to topography and underlying material in the Baxter-Hammack-Loring general soil map unit (Soil Survey of Livingston County, Kentucky; September 1993).

13. KY-2012-02-01-05 | Livingston County - September 1993

    Relationship of soils to topography and underlying material in the Loring-Brandon-Saffell general soil map unit (Soil Survey of Livingston County, Kentucky; September 1993).

14. KY-2012-02-01-54 | Simpson County - May 1985

    Relationship of soils to topography and underlying material in the Mountview-Baxter general soil map unit (Soil Survey of Simpson County, Kentucky; May 1985).

15. KY-2012-02-01-55 | Simpson County - May 1985

    Relationship of soils to topography and underlying material in the Nicholson-Lawrence-Robertsville general soil map unit (Soil Survey of asdSimpson County, Kentucky; May 1985).f

16. KY-2012-02-01-59 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Fredonia-Pembroke-Caneyville map unit (Soil Survey of Todd County, Kentucky; September 1987).

17. KY-2012-02-01-61 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Hammack-Baxter-Crider map unit (Soil Survey of Todd County, Kentucky; September 1987).

18. KY-2012-02-01-62 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Pembroke-Vertrees map unit (Soil Survey of Todd County, Kentucky; September 1987).

19. KY-2012-02-01-69 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Decatur-Bewleyville-Clarksville general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

20. OK-2012-02-16-06 | Cherokee and Delaware Counties - December 1970

    Major soils in soil associations 1 and 3 and their relation to the landscape. Soil association 1 is near the middle of the figure, and soil association 3 is to the left (Soil Survey of Cherokee and Delaware Counties, Oklahoma; December 1970).

21. OK-2012-02-17-20 | Ottawa County - November 1964

    Major soil series in soil associations 6 and 7, and their relation to the landscape. Typical slope range is shown for the soil series (Soil Survey of Ottawa County, Oklahoma; November 1964).

22. TN-2012-03-19-30 | Warren County - September 1967

    Major and minor soils and underlying parent material in the Dickson-Mountview association (Soil Survey of Warren County, TN; 1967).

23. TN-2012-03-19-31 | Warren County - September 1967

    Major and minor soils and underlying parent materials in the Baxter-Mountview association (Soil Survey of Warren County, TN; 1967).

24. TN-2012-03-19-32 | Warren County - September 1967

    Major and minor soils and underlying parent materials in the Waynesboro-Cumberland association (Soil Survey of Warren County, TN; 1967).

25. TN-2012-03-19-38 | Williamson County - August 1964

    Major and minor soils and underlying parent materials in the Mountview-Baxter-Bodine association (Soil Survey of Williamson County, TN; 1964).

Map Units

Map units containing BAXTER as a major component. Limited to 250 records.

Map Unit Name	Symbol	Map Unit Area (ac)	Map Unit Key	National Map Unit Symbol	Soil Survey Area	Publication Date	Map Scale
Baxter cherty silt loam, hilly phase	Bc	980	330082	c2gt	al079	1950	1:20000
Baxter (Fullerton) gravelly silt loam, 6 to 12 percent slopes, eroded	Bb	356	330081	2ykcq	al079	1950	1:20000
Baxter (Fullerton) gravelly silt loam, 6 to 12 percent slopes, eroded	Bsn	12149	522726	2ykcq	al083	1953	1:20000
Baxter cherty silt loam steep phase	Bsz	10618	522729	kjy7	al083	1953	1:20000
Baxter cherty silt loam hilly phase	Bsl	10494	522725	kjy3	al083	1953	1:20000
Baxter cherty silt loam eroded hilly phase	Bsh	8452	522724	kjy2	al083	1953	1:20000
Baxter cherty silty clay loam severely eroded rolling phase	Bxd	3487	522730	kjy8	al083	1953	1:20000
Baxter cherty silt loam eroded steep phase	Bsf	1996	522723	kjy1	al083	1953	1:20000
Baxter (Fullerton) gravelly silt loam, 6 to 12 percent slopes	Bso	1845	522727	2ykcp	al083	1953	1:20000
Baxter cherty silty clay loam severely eroded hilly phase	Bxr	1218	522731	kjy9	al083	1953	1:20000
Baxter (Fullerton) gravelly silt loam, 6 to 12 percent slopes, eroded	Bd	11918	523074	2ykcq	al089	1958	1:24000
Baxter cherty silty clay loam, severely eroded, rolling	Bh	5026	523078	kk9h	al089	1958	1:24000
Baxter (Fullerton) gravelly silt loam, 6 to 12 percent slopes	Bc	1378	523073	2ykcp	al089	1958	1:24000
Baxter cherty silt loam, eroded, hilly	Bf	1124	523076	kk9f	al089	1958	1:24000
Baxter cherty silty clay loam, severely eroded, hilly	Bk	722	523079	kk9j	al089	1958	1:24000
Baxter cherty silt loam, hilly	Be	402	523075	kk9d	al089	1958	1:24000
Baxter cherty silty clay loam, severely eroded, undulating	Bg	400	523077	kk9g	al089	1958	1:24000
Baxter very gravelly silt loam, 20 to 45 percent slopes	BaF	10131	566563	m0k7	ar143	1966	1:20000
Baxter very gravelly silt loam, 12 to 20 percent slopes	BaE	1673	566562	m0k6	ar143	1966	1:20000
Baxter very gravelly silt loam, 8 to 12 percent slopes	BaD	1125	566561	m0k5	ar143	1966	1:20000
Baxter very gravelly silt loam, 3 to 8 percent slopes	BaC	601	566560	m0k4	ar143	1966	1:20000
Alford-Baxter complex, 18 to 35 percent slopes	954F	3947	713954	ryxs	il069	2003	1:12000
Baxter gravelly silt loam, 18 to 35 percent slopes	599F	3232	713940	ryxb	il069	2003	1:12000
Baxter gravelly silt loam, 35 to 70 percent slopes	599G	320	713941	ryxc	il069	2003	1:12000
Baxter gravelly silt loam, 10 to 18 percent slopes	599D	65	713939	ryx9	il069	2003	1:12000
Alford-Baxter complex, 10 to 18 percent slopes, eroded	954D2	26	713953	ryxr	il069	2003	1:12000
Alford-Baxter complex, 10 to 18 percent slopes, eroded	954D2	190	608752	nfg5	il151	2003	1:12000
Alford-Baxter complex, 18 to 35 percent slopes	954F	48	608140	ndtf	il151	2003	1:12000
Baxter gravelly silt loam, 18 to 35 percent slopes	599F	15	608145	ndtl	il151	2003	1:12000
Menfro-Baxter complex, 10 to 18 percent slopes, eroded	694D2	88	748924	t49v	il153	2004	1:12000
Menfro-Baxter complex, 18 to 35 percent slopes	694F	56	748925	t49w	il153	2004	1:12000
Menfro-Baxter complex, 18 to 35 percent slopes	694F	1577	199468	6pkg	il181	2001	1:12000
Menfro-Baxter complex, 10 to 18 percent slopes, eroded	694D2	328	199469	6pkh	il181	2001	1:12000
Menfro-Baxter complex, 10 to 18 percent slopes	694D	30	199465	6pkc	il181	2001	1:12000
Frederick-Baxter variant complex, karst, 4 to 12 percent slopes, eroded	FxC2	927	535483	kz6n	in175	1984	1:15840
Crider-Baxter complex, 12 to 30 percent slopes, severely eroded	CtE3	8302	1404746	1j4rd	ky033	2005	1:12000
Hammack-Baxter complex, 6 to 12 percent slopes	HbC	7527	549059	lfbl	ky047	1977	1:20000
Hammack-Baxter complex, 6 to 12 percent slopes, severely eroded	HbC3	4732	549060	lfbm	ky047	1977	1:20000
Hammack-Baxter complex, 2 to 6 percent slopes	HbB	4108	549058	lfbk	ky047	1977	1:20000
Baxter gravelly silt loam, 12 to 20 percent slopes	BaD	1722	549037	2xv21	ky047	1977	1:20000
Baxter gravelly silt loam, 20 to 30 percent slopes	BaE	376	549038	2xv23	ky047	1977	1:20000
Baxter gravelly silt loam, 20 to 50 percent slopes	BaE	11258	549095	2xv25	ky055	1985	1:20000
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	645	549643	lfyf	ky085	1967	1:20000
Baxter cherty silty clay loam, 6 to 12 percent slopes, severely eroded	BcC3	415	549642	lfyd	ky085	1967	1:20000
Baxter gravelly silt loam, 20 to 50 percent slopes	BaE	7019	549304	2xv25	ky139	1989	1:20000
Baxter gravelly silt loam, 6 to 12 percent slopes	BaC	5426	548689	2xv1z	ky141	1972	1:20000
Baxter gravelly silt loam, 12 to 20 percent slopes	BaD	2884	548690	2xv21	ky141	1972	1:20000
Baxter cherty silty clay loam, 6 to 12 percent slopes, severely eroded	BbC3	1247	548691	ldyq	ky141	1972	1:20000
Baxter gravelly silt loam, 6 to 12 percent slopes, eroded	BaC2	20238	549711	2xv20	ky169	1965	1:15840
Baxter gravelly silt loam, 12 to 20 percent slopes, eroded	BaD2	14120	549713	2xv22	ky169	1965	1:15840
Baxter gravelly silt loam, 20 to 30 percent slopes, eroded	BaE2	8355	549715	2xv24	ky169	1965	1:15840
Baxter gravelly silt loam, 2 to 6 percent slopes	BaB	5716	549708	2xv1x	ky169	1965	1:15840
Baxter gravelly silt loam, 20 to 30 percent slopes	BaE	2886	549714	2xv23	ky169	1965	1:15840
Baxter gravelly silt loam, 12 to 20 percent slopes	BaD	1845	549712	2xv21	ky169	1965	1:15840
Baxter gravelly silt loam, 2 to 6 percent slopes, eroded	BaB2	1695	549709	2xv1y	ky169	1965	1:15840
Baxter gravelly silt loam, 6 to 12 percent slopes	BaC	1693	549710	2xv1z	ky169	1965	1:15840
Baxter-Talbott rocky silt loams, 20 to 30 percent slopes, eroded (baxter, caneyville rocky)	BeE2	1581	549721	lg0y	ky169	1965	1:15840
Baxter-Talbott rocky silt loams, 12 to 20 percent slopes, eroded (baxter, caneyville rocky)	BeD2	1081	549720	lg0x	ky169	1965	1:15840
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	932	549717	lg0t	ky169	1965	1:15840
Baxter cherty silty clay loam, 20 to 30 percent slopes, severely eroded	BcE3	605	549718	lg0v	ky169	1965	1:15840
Baxter-Talbott rocky silty clay loams, 12 to 20 percent slopes, severely eroded (baxter, caneyville rocky)	BfD3	570	549722	lg0z	ky169	1965	1:15840
Baxter cherty silty clay loam, 6 to 12 percent slopes, severely eroded	BcC3	530	549716	lg0s	ky169	1965	1:15840
Baxter-Talbott rocky silt loams, 6 to 12 percent slopes, eroded (baxter, caneyville rocky)	BeC2	515	549719	lg0w	ky169	1965	1:15840
Baxter cherty silt loam, 12 to 20 percent slopes	BaD	2150	549928	lg7m	ky179	1967	1:15840
Cumberland cherty silt loam, 6 to 12 percent slopes (baxter)	CvC	3344	552390	ljt1	ky199	1969	1:12000
Cumberland cherty silt loam, 12 to 20 percent slopes (baxter)	CvD	1779	552391	ljt2	ky199	1969	1:12000
Cumberland cherty silty clay loam, 12 to 20 percent slopes, severely eroded (baxter)	CwD3	1165	552392	ljt3	ky199	1969	1:12000
Etowah cherty silt loam, 6 to 12 percent slopes (baxter)	EtC	1136	552397	ljt8	ky199	1969	1:12000
Etowah cherty silt loam, 2 to 6 percent slopes (baxter)	EtB	704	552396	ljt7	ky199	1969	1:12000
Cumberland cherty silt loam, 2 to 6 percent slopes (baxter)	CvB	379	552389	ljt0	ky199	1969	1:12000
Baxter gravelly silt loam, 6 to 12 percent slopes	BaC	25812	549790	2xv1z	ky213	1982	1:20000
Baxter gravelly silt loam, 12 to 20 percent slopes	BaD	10640	549791	2xv21	ky213	1982	1:20000
Baxter gravelly silt loam, 2 to 6 percent slopes	BaB	3995	549789	2xv1x	ky213	1982	1:20000
Baxter gravelly silt loam, 20 to 30 percent slopes	BaE	2270	549792	2xv23	ky213	1982	1:20000
Hammack-Baxter complex, 6 to 12 percent slopes, eroded	HbC2	4830	551162	lhjf	ky219	1984	1:20000
Hammack-Baxter complex, 2 to 6 percent slopes	HbB	1290	551161	lhjd	ky219	1984	1:20000
Baxter gravelly silt loam, 12 to 20 percent slopes	BaD	650	551142	2xv21	ky219	1984	1:20000
Hammack-Baxter complex, 6 to 12 percent slopes, severely eroded	HbC3	450	551163	lhjg	ky219	1984	1:20000
Baxter gravelly silt loam, 6 to 12 percent slopes	BaC	39522	553843	2xv1z	ky227	2004	1:12000
Baxter gravelly silt loam, 12 to 20 percent slopes	BaD	34401	553844	2xv21	ky227	2004	1:12000
Baxter gravelly silt loam, 20 to 30 percent slopes	BaE	4269	553845	2xv23	ky227	2004	1:12000
Baxter gravelly silt loam, 2 to 6 percent slopes	BaB	2525	553842	2xv1x	ky227	2004	1:12000
Baxter gravelly silty clay loam, 6 to 12 percent slopes, severely eroded	BbC3	2122	553846	llb0	ky227	2004	1:12000
Baxter-Urban land complex, 6 to 12 percent slopes	BrC	762	553814	ll8z	ky227	2004	1:12000
Baxter gravelly silty clay loam, 12 to 20 percent slopes, severely eroded	BbD3	725	553847	llb1	ky227	2004	1:12000
Baxter-Urban land complex, 12 to 20 percent slopes	BrD	372	553813	ll8y	ky227	2004	1:12000
Baxter-Urban land complex, 2 to 6 percent slopes	BrB	291	553812	ll8x	ky227	2004	1:12000
Clarksville-Baxter cobbly silt loams, 4 to 12 percent slopes	CxC	4246	550065	lgd1	ky231	1985	1:20000
Clarksville-Baxter cobbly silt loams, 12 to 20 percent slopes	CxD	1898	550066	lgd2	ky231	1985	1:20000
Hammack-Baxter complex, karst, 6 to 12 percent slopes, eroded	HbC2	23585	549588	lfwn	ky607	1992	1:20000
Baxter very gravelly silt loam, karst, 12 to 20 percent slopes, eroded	BaD2	14946	549555	lfvl	ky607	1992	1:20000
Baxter very gravelly silt loam, karst, 6 to 12 percent slopes, eroded	BaC2	7436	549554	lfvk	ky607	1992	1:20000
Baxter very gravelly silty clay loam, karst, 12 to 20 percent slopes, severely eroded	BbD3	5814	549558	lfvp	ky607	1992	1:20000
Baxter very gravelly silty clay loam, karst, 6 to 12 percent slopes, severely eroded	BbC3	3351	549557	lfvn	ky607	1992	1:20000
Hammack-Baxter complex, karst, 6 to 12 percent slopes, severely eroded	HbC3	3243	549589	lfwp	ky607	1992	1:20000
Baxter soils, karst, 12 to 20 percent slopes, very severely eroded	BeD4	977	549560	lfvr	ky607	1992	1:20000
Baxter soils, karst, 6 to 12 percent slopes, very severely eroded	BeC4	698	549559	lfvq	ky607	1992	1:20000
Baxter very gravelly silt loam, karst, 20 to 30 percent slopes, eroded	BaE2	639	549556	lfvm	ky607	1992	1:20000
Baxter very gravelly silt loam, karst, 2 to 6 percent slopes, eroded	BaB2	146	549553	lfvj	ky607	1992	1:20000
Baxter-Hammack complex, 20 to 30 percent slopes	BaE	55000	549445	lfr1	ky629	1979	1:20000
Hammack-Baxter complex, 6 to 12 percent slopes	HxC	47580	549467	lfrr	ky629	1979	1:20000
Hammack-Baxter complex, 12 to 20 percent slopes	HxD	31360	549469	lfrt	ky629	1979	1:20000
Hammack-Baxter complex, 6 to 12 percent slopes, severely eroded	HxC3	9000	549468	lfrs	ky629	1979	1:20000
Hammack-Baxter complex, 12 to 20 percent slopes, severely eroded	HxD3	8200	549470	lfrv	ky629	1979	1:20000
Baxter-Hammack complex, 30 to 60 percent slopes	BaF	3780	549446	lfr2	ky629	1979	1:20000
Baxter gravelly silt loam, 6 to 12 percent slopes, eroded	BaC2	22675	2452945	2xv20	ky646	1966	1:15840
Cumberland cherty silt loam, 2 to 6 percent slopes, eroded (baxter)	CtB2	18422	2452970	2nbj2	ky646	1966	1:15840
Baxter gravelly silt loam, 12 to 20 percent slopes, eroded	BaD2	17964	2452946	2xv22	ky646	1966	1:15840
Cumberland cherty silt loam, 6 to 12 percent slopes, eroded (baxter)	CtC2	13625	2452971	2nbj3	ky646	1966	1:15840
Baxter gravelly silt loam, 20 to 30 percent slopes, eroded	BaE2	5897	2452947	2xv24	ky646	1966	1:15840
Baxter gravelly silt loam, 2 to 6 percent slopes	BaB	5235	2452944	2xv1x	ky646	1966	1:15840
Cumberland cherty silty clay, 6 to 12 percent slopes, severely eroded (baxter)	CuC3	3267	2452973	2nbj5	ky646	1966	1:15840
Cumberland cherty silt loam, 12 to 20 percent slopes, eroded (baxter)	CtD2	3094	2452972	2nbj4	ky646	1966	1:15840
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	2966	2452948	2nbhc	ky646	1966	1:15840
Cumberland cherty silty clay, 12 to 20 percent slopes, severely eroded (baxter)	CuD3	1787	2452974	2nbj6	ky646	1966	1:15840
Baxter gravelly silt loam, 6 to 12 percent slopes, eroded	BaC2	15470	2453051	2xv20	ky647	1989	1:20000
Baxter gravelly silt loam, 12 to 20 percent slopes, eroded	BaD2	9679	2453052	2xv22	ky647	1989	1:20000
Baxter gravelly silt loam, 2 to 6 percent slopes	BaB	5426	2453050	2xv1x	ky647	1989	1:20000
Baxter gravelly silt loam, 20 to 30 percent slopes	BaE	1011	2453053	2xv23	ky647	1989	1:20000
Baxter gravelly silt loam, 12 to 20 percent slopes, eroded	BaD2	3210	2452831	2xv22	ky709	1995	1:20000
Baxter gravelly silt loam, 6 to 12 percent slopes, eroded	BaC2	3109	2452830	2xv20	ky709	1995	1:20000
Baxter gravelly silt loam, 2 to 6 percent slopes	BaB	161	2452829	2xv1x	ky709	1995	1:20000
Baxter gravelly silt loam, 20 to 30 percent slopes	BaE	94	2452832	2xv23	ky709	1995	1:20000
Baxter cherty silty clay loam, severely eroded, sloping phase	Bg	1468	524863	km52	tn031	1956	1:20000
Baxter cherty silt loam, gently sloping phase	Ba	1230	524857	km4w	tn031	1956	1:20000
Baxter cherty silty clay loam, severely eroded, strongly sloping phase	Bh	676	524864	km53	tn031	1956	1:20000
Baxter cherty silty clay loam, severely eroded, gently sloping phase	Bf	127	524862	km51	tn031	1956	1:20000
Baxter cherty silt loam, eroded rolling phase	Be	10197	527143	kpjm	tn051	1950	1:20000
Baxter cherty silt loam, rolling phase	Bd	4131	527142	kpjl	tn051	1950	1:20000
Baxter cherty silt loam, eroded hilly phase	Bg	2590	527145	kpjp	tn051	1950	1:20000
Baxter cherty silty clay loam, severely eroded rolling phase	Bm	2517	527148	kpjs	tn051	1950	1:20000
Baxter cherty silt loam, eroded undulating phase	Bc	2047	527141	kpjk	tn051	1950	1:20000
Baxter cherty silt loam, eroded steep phase	Bk	1967	527147	kpjr	tn051	1950	1:20000
Baxter cherty silty clay loam, severely eroded steep phase	Bo	1957	527150	kpjv	tn051	1950	1:20000
Baxter cherty silty clay loam, severely eroded hilly phase	Bn	1783	527149	kpjt	tn051	1950	1:20000
Baxter cherty silt loam, hilly phase	Bf	1710	527144	kpjn	tn051	1950	1:20000
Baxter cherty silt loam, steep phase	Bh	1608	527146	kpjq	tn051	1950	1:20000
Baxter cherty silt loam, undulating phase	Bb	608	527140	kpjj	tn051	1950	1:20000
Mountview silt loam, rolling shallow phase	Mk	7115	527536	kpy9	tn083	1952	1:20000
Mountview silt loam, hilly shallow phase	Mm	6836	527538	kpyc	tn083	1952	1:20000
Mountview silt loam, eroded hilly shallow phase	Mn	5873	527539	kpyd	tn083	1952	1:20000
Mountview silt loam, eroded, rolling shallow phase	Ml	4309	527537	kpyb	tn083	1952	1:20000
Mountview silty clay loam, severely eroded hilly shallow phase	Mr	1067	527542	kpyh	tn083	1952	1:20000
Stony steep land, Baxter soil material	Sa	833	527550	kpyr	tn083	1952	1:20000
Mountview silty clay loam, severely eroded rolling phase	Mo	561	527540	kpyf	tn083	1952	1:20000
Mountview silty clay loam, severely eroded rolling shallow phase	Mp	332	527541	kpyg	tn083	1952	1:20000
Baxter cherty silty clay loam, severely eroded hilly phase	Bg	214	527506	kpxb	tn083	1952	1:20000
Baxter cherty silt loam	Bs	3539	527559	kpz1	tn085	1943	1:20000
Rough stony land, Baxter soil material	RsB	34	527587	kpzy	tn085	1943	1:20000
Baxter cherty silt loam, eroded moderately steep phase	Be	1191	527603	kq0g	tn099	1955	1:20000
Baxter cherty silt loam, eroded sloping phase	Bc	956	527601	kq0d	tn099	1955	1:20000
Baxter cherty silty clay loam, severely eroded sloping phase	Br	914	527612	kq0r	tn099	1955	1:20000
Baxter cherty silt loam, moderately steep phase	Bd	890	527602	kq0f	tn099	1955	1:20000
Baxter cherty silt loam, eroded gently sloping phase	Ba	539	527599	kq0b	tn099	1955	1:20000
Baxter cherty silty clay loam, severely eroded moderately steep phase	Bs	519	527613	kq0s	tn099	1955	1:20000
Baxter cherty silt loam, sloping phase	Bb	418	527600	kq0c	tn099	1955	1:20000
Mountview silt loam, eroded, sloping shallow phase	Mu	4070	527824	kq7l	tn119	1955	1:20000
Mountview silt loam, sloping shallow phase	Mt	1131	527823	kq7k	tn119	1955	1:20000
Mountview silty clay loam, severely eroded sloping shallow phase	Mv	678	527825	kq7m	tn119	1955	1:20000
Baxter cherty silt loam, 20 to 35 percent slopes	BaE	21509	527965	kqd4	tn125	1972	1:15840
Baxter soils and rock outcrop, 20 to 45 percent slopes	BkF	6230	527969	kqd8	tn125	1972	1:15840
Baxter soils, 12 to 25 percent slopes, severely eroded	BgE3	1459	527968	kqd7	tn125	1972	1:15840
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	6939	528150	kql3	tn147	1965	1:15840
Baxter cherty silty clay loam, 5 to 12 percent slopes severely eroded	BcC3	6524	528149	kql2	tn147	1965	1:15840
Baxter cherty silt loam, 20 to 30 percent slopes	BaE	3873	528147	kql0	tn147	1965	1:15840
Baxter very rocky soils, 20 to 30 percent slopes	BkE	1584	528153	kql6	tn147	1965	1:15840
Baxter cherty silt loam, 2 to 5 percent slopes	BaB	830	528144	kqkx	tn147	1965	1:15840
Baxter very rocky soils, 12 to 20 percent slopes	BkD	338	528152	kql5	tn147	1965	1:15840
Hammack-Baxter complex, 12 to 20 percent slopes	HxD	125	3160466	1v6bm	tn161	1953	1:20000
Baxter-Hammack complex, 20 to 30 percent slopes	BaE	67	3160463	1v6bb	tn161	1953	1:20000
Hammack-Baxter complex, 6 to 12 percent slopes	HxC	21	3160465	1v6bk	tn161	1953	1:20000
Baxter cherty silt loam, 20 to 30 percent slopes	BaE	4679	529858	ksc6	tn177	1965	1:15840
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	1917	529861	ksc9	tn177	1965	1:15840
Baxter cherty silty clay loam, 5 to 12 percent slopes, severely eroded	BcC3	831	529860	ksc8	tn177	1965	1:15840
Mountview silt loam, shallow, 5 to 12 percent slopes, eroded	MvC2	9212	523573	kktg	tn187	1961	1:15840
Mountview silt loam, shallow, 5 to 12 percent slopes	MvC	8001	523572	kktf	tn187	1961	1:15840
Mountview silt loam, shallow, 2 to 5 percent slopes, eroded	MvB2	2822	523571	kktd	tn187	1961	1:15840
Baxter cherty silt loam, 20 to 30 percent slopes	BaE	2052	523466	kkq0	tn187	1961	1:15840
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	1473	523468	kkq2	tn187	1961	1:15840
Mountview silt loam, shallow, 12 to 20 percent slopes	MvD	934	523575	kktj	tn187	1961	1:15840
Mountview silt loam, shallow, 2 to 5 percent slopes	MvB	805	523570	kktc	tn187	1961	1:15840
Mountview silt loam, shallow, 12 to 20 percent slopes, eroded	MvD2	770	523576	kktk	tn187	1961	1:15840
Mountview silt loam, shallow, 5 to 12 percent slopes, severely eroded	MvC3	646	523574	kkth	tn187	1961	1:15840
Baxter cherty silty clay loam, 5 to 12 percent slopes, severely eroded	BcC3	453	523467	kkq1	tn187	1961	1:15840
Baxter cherty silt loam, 20 to 30 percent slopes	BaE	2770	2427397	2mgx4	tn610	1960	1:15840
Baxter cherty silty clay loam, 12 to 20 percent slopes, severely eroded	BcD3	611	2427398	2mgx5	tn610	1960	1:15840
Christian-Baxter complex, 5 to 20 percent slopes, eroded	CbD2	29050	2439168	2mw4v	tn701	1985	1:24000

Map of Series Extent

Approximate geographic distribution of the BAXTER soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry (updated 2023-10-04).